Fig. 8.From: Source process of the 2011 off the Pacific coast of Tohoku Earthquake inferred from waveform inversion with long-period strong-motion recordsMoment rate as a function of time and distance from the rupture starting point. The moment rate at each mesh is shown with an interval of 2.5 s in time and 15 km in distance. FTWTV of 2.5 km/s (no moment releases before this line) is indicated by the dotted line. Dashed lines show the apparent rupture velocity of 3.5 km/s.Back to article page